The distribution and activity of saprophytic, cellulolytic, sulfate-re
ducing, and methanogenic bacteria was studied in bottom sediments of L
ake Michigan and Green Bay. Maximal abundance of these bacteria was fo
und in the upper horizons of the sediments. The intensity of cellulose
decomposition and sulfate reduction declined toward the lower horizon
s; on the contrary, the rates of acetate and methane formation increas
ed. The maximum rate of Mn4+ reduction was recorded in the under-surfa
ce layers.